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    Lessons From Oedometer Tests on High Quality Samples

    Source: Journal of Geotechnical Engineering:;1986:;Volume ( 112 ):;issue: 008
    Author:
    R. D. Holtz
    ,
    M. B. Jamiolkowski
    ,
    R. Lancellotta
    DOI: 10.1061/(ASCE)0733-9410(1986)112:8(768)
    Publisher: American Society of Civil Engineers
    Abstract: A well planned and carefully executed program of oedometer tests on high quality undisturbed samples is shown to provide considerable practical information about the soil properties of a natural, very stiff clay deposit. The effects of sample disturbance and type of oedometer on the preconsolidation stress are shown. A special long‐term oedometer test verified earlier results that
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      Lessons From Oedometer Tests on High Quality Samples

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/19923
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    • Journal of Geotechnical Engineering

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    contributor authorR. D. Holtz
    contributor authorM. B. Jamiolkowski
    contributor authorR. Lancellotta
    date accessioned2017-05-08T20:34:19Z
    date available2017-05-08T20:34:19Z
    date copyrightAugust 1986
    date issued1986
    identifier other%28asce%290733-9410%281986%29112%3A8%28768%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/19923
    description abstractA well planned and carefully executed program of oedometer tests on high quality undisturbed samples is shown to provide considerable practical information about the soil properties of a natural, very stiff clay deposit. The effects of sample disturbance and type of oedometer on the preconsolidation stress are shown. A special long‐term oedometer test verified earlier results that
    publisherAmerican Society of Civil Engineers
    titleLessons From Oedometer Tests on High Quality Samples
    typeJournal Paper
    journal volume112
    journal issue8
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1986)112:8(768)
    treeJournal of Geotechnical Engineering:;1986:;Volume ( 112 ):;issue: 008
    contenttypeFulltext
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